@article {Tombrou200761,
	title = {Model evaluation of the atmospheric boundary layer and mixed-layer evolution},
	journal = {Boundary-Layer Meteorology},
	volume = {124},
	number = {1},
	year = {2007},
	note = {cited By (since 1996)10},
	pages = {61-79},
	abstract = {In the present study, an attempt is made to assess the atmospheric boundary-layer (ABL) depth over an urban area, as derived from different ABL schemes employed by the mesoscale model MM5. Furthermore, the relationship of the mixing height, as depicted by the measurements, to the calculated ABL depth or other features of the ABL structure, is also examined. In particular, the diurnal evolution of ABL depth is examined over the greater Athens area, employing four different ABL schemes plus a modified version, whereby urban features are considered. Measurements for two selected days, when convective conditions prevailed and a strong sea-breeze cell developed, were used for comparison. It was found that the calculated eddy viscosity profile seems to better indicate the mixing height in both cases, where either a deep convective boundary layer develops, or a more confined internal boundary layer is formed. For the urban scheme, the incorporation of both anthropogenic and storage heat release provides promising results for urban applications. {\textcopyright} Springer Science+Business Media, B.V. 2007.},
	keywords = {aerodynamics, Atmospheric boundary layer, boundary layer, Boundary layers, eddy, Eddy viscosity, entrainment, Entrainment layer, Mathematical models, mesoscale meteorology, Mesoscale model, Meteorology, mixed layer, mixing, Mixing height, model validation, sea breeze, urban area, Viscosity, viscous flow, wind},
	issn = {00068314},
	doi = {10.1007/s10546-006-9146-5},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-34250218167\&partnerID=40\&md5=e296cd837cefd3097bfba8d34b58c586},
	author = {Tombrou, M.a and Dandou, A.a and Helmis, C.a and Akylas, E.b and Angelopoulos, G.a and H. A. Flocas and Assimakopoulos, V.b and Soulakellis, N.c}
}
